O papel das nuvens rasas no transporte de vapor d’água
A mesoscale model was evaluated in this work in order to represent the vertical transport of water vapor by shallow cumulus. The results confirmed the efficiency of shallow cumulus, triggered by surface heating, on the vertical transport of water vapor to above boundary layer levels.
Spremljeno u:
| Izdano u: | Ciência e Natura |
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| Glavni autori: | , , , , , |
| Format: | Artigo |
| Jezik: | Português |
| Izdano: |
Universidade Federal de Santa Maria
2011
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| Teme: | |
| Online pristup: | https://www.redalyc.org/articulo.oa?id=467546167062 |
| Oznake: |
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